Abstract:The erosion of perfectly brittle materials under low-speed impacts is studied by the combination of the Hertzian contact theory and the maximum stress criterion. It is found that the fractional erosion per impact is proportional to the product of the square root of the yield strain and the ratio of the kinetic energy per volume of the impacting body to the critical strain energy density of the target. The novel formula is conceptually extended to the erosion of cracked brittle materials.
“…Considering the perpendicular collision between a rigid sphere and a brittle half-space, the stress field within the half-space is determined by the Hertzian contact theory (Barber, 2018). Whether or not soil breaks at any spatial point can be judged the maximum stress criterion, the eroded volume V per impact is written as (Wang, 2020),…”
Section: Theoretical Modelmentioning
confidence: 99%
“…Considering the perpendicular collision between a rigid sphere and a brittle half‐space, the stress field within the half‐space is determined by the Hertzian contact theory (Barber, 2018). Whether or not soil breaks at any spatial point can be judged the maximum stress criterion, the eroded volume per impact is written as (Wang, 2020),where is a constant; , , are the density, diameter, impact speed of one saltator, respectively; and are the yield strength and Young's modulus of soil, respectively. Soil aggregation could be eroded or crushed when it strikes with the land surface.…”
Wind erosion is a physical process predominated by airborne grains rather than the wind itself. The soil deformation is either elastic–plastic or fully plastic during its collisions with solid grains, corresponding to dense and loose soils, respectively. Only the fully plastic deformation was previously taken into account in the physically‐based wind erosion models. The impact erosion of dry and dense soil surface can be well quantified by the contact mechanics and strength theories. In this study, with the help of Owen's uniform saltation model, a simple expression for wind erosion rate is derived based upon the eroded volume per impact when soil deforms in the elastic–plastic manner. The new expression, a simple analytical function of several conventional variables and parameters of wind and soil, describes the effects of saltation flux and soil susceptibility. Its validity is verified by some field and laboratory experiments.
“…Considering the perpendicular collision between a rigid sphere and a brittle half-space, the stress field within the half-space is determined by the Hertzian contact theory (Barber, 2018). Whether or not soil breaks at any spatial point can be judged the maximum stress criterion, the eroded volume V per impact is written as (Wang, 2020),…”
Section: Theoretical Modelmentioning
confidence: 99%
“…Considering the perpendicular collision between a rigid sphere and a brittle half‐space, the stress field within the half‐space is determined by the Hertzian contact theory (Barber, 2018). Whether or not soil breaks at any spatial point can be judged the maximum stress criterion, the eroded volume per impact is written as (Wang, 2020),where is a constant; , , are the density, diameter, impact speed of one saltator, respectively; and are the yield strength and Young's modulus of soil, respectively. Soil aggregation could be eroded or crushed when it strikes with the land surface.…”
Wind erosion is a physical process predominated by airborne grains rather than the wind itself. The soil deformation is either elastic–plastic or fully plastic during its collisions with solid grains, corresponding to dense and loose soils, respectively. Only the fully plastic deformation was previously taken into account in the physically‐based wind erosion models. The impact erosion of dry and dense soil surface can be well quantified by the contact mechanics and strength theories. In this study, with the help of Owen's uniform saltation model, a simple expression for wind erosion rate is derived based upon the eroded volume per impact when soil deforms in the elastic–plastic manner. The new expression, a simple analytical function of several conventional variables and parameters of wind and soil, describes the effects of saltation flux and soil susceptibility. Its validity is verified by some field and laboratory experiments.
“…The study of the movement patterns of solid particles in the liquid–solid two-phase flow field, the mutual impact process between the particles and the heat exchange surface, and the erosion patterns is of great significance to guide the design and operation of the equipment and, consequently, to reduce wear effectively. The studies on the erosion characteristics of liquid–solid two-phase have proliferated, primarily focusing on the particle size, , particle morphology, , particle and target hardness, particle impact angle , and velocity, , temperature, , development of erosion models and numerical simulation frameworks, − etc. In recent years, with the rapid development of computer technology and testing techniques, the study of liquid–solid two-phase erosion characteristics has gradually moved from macroscopic to microscopic.…”
The erosion of the dimple walls is investigated experimentally and numerically. A mathematical simulation framework was proposed to describe quantitatively the morphological evolution of the dimple wall quantitatively. As the wall shape continues to evolve, the wall shear stress, mesh deformation, and erosion rate would decrease and gradually tend to be constant. Two distinct regions have been identified along the dimple's windward wall surface: the wall's central area and the lateral area. In the central region, the wall profile flare occurs mainly in the early stage. In the lateral region, profile flare occurs mainly in the later stages of erosion. The microhardness of the wall surface shows a positive correlation with the erosion rate. The liquid−solid two-phase impinges on the wall at a smaller angle, and the wall material removal process is mainly based on the microcutting and slip mechanism. The results provide theoretical implications for the design of dimple-shaped, wide-channel welded plate heat exchangers.
“…O'Brien and McKenna Neuman (2019) measured even lower impact speeds, which they assert may be due to the high resolution of their PTV system, allowing them to sample down to a distance only 50 μm above the bed surface. In comparison, Wang (2020) reports that the threshold impact speed required to cause an abrasion event (i.e., a singular impact by the particle on the target rock) is only 0.025 m s −1 and 0.094 m s −1 , for basalt and rhyolite, respectively. This would suggest that abrasion can occur under most saltation conditions.…”
Ventifacts are rocks that have been shaped through abrasion by wind‐transported sediment. Their surfaces may be ornamented with characteristic microscale features that are replicated and overlain to form complex patterns. Compared to a large body of work on the transport of unconsolidated sediment in which the atmospheric boundary‐layer flow and sand cloud respond to perturbations in the developing topography, no experimental work to this date has addressed morphodynamic feedback at the particle scale in aeolian systems dominated by abrasion. This article reports on a case study in which laser Doppler anemometry was used in wind tunnel experiments to measure air flow and sand transport over a highly ornamented, tabular ventifact from the Taylor Valley, Antarctica. Periodicity characterizing the static microtopography of the ventifact was observed to be strongly imprinted on the kinetics of both the airflow and particle cloud when sampled along a transect of the ventifact aligned with flow in the wind tunnel matching the dominant sand transporting wind direction for the ventifact in situ. The vertical velocity component was especially well synchronized, with changes in elevation on the order of 2–4 mm. The horizontal component of particle velocity demonstrated an offset in the downwind direction associated with the large forward momentum of the saltating sand particles. However, submillimeter relief on the fixed ventifact surface was not sufficient to initiate kinetic feedback, as observed along a transect aligned normal to a series of elongated flute structures and the dominant sand transporting wind direction. The particle‐scale experimental results confirm that (i) abrasion of this ventifact principally occurred under a unimodal wind and sand transport regime of low‐moderate intensity, and (ii) relief arising from weathering, as governed by the ventifact's lithology, likely initiated development of the present‐day ornamentation.
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